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红色泥岩
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  red mudstone
     This paper mainly presents the relations among moisture content density and claygrain content of pebble soil mass of weathered red mudstone of Badong Formation,Middle Trias.
     研究了巴东组红色泥岩风化含砾粘土的含水量、密度及粘粒含量与内聚力C、摩擦角的关系。
短句来源
     RESEARCH ON THE RELATIVITY BETWEEN THE STRENGTH OF RED MUDSTONE WEATHERED PEBBLE SOIL AND PHYSICAL CHARACTERS
     红色泥岩风化含砾粘土的抗剪强度参数与物理性质相关性研究
短句来源
     The play is composed of Triassic-Jurassic source rock, Tertiary-Neogene, Cretaceous and Jurassic sandstone reservoir rock, and the seal rocks of regional Jurassic red mudstone and Tertiary-Neogene's salty gypseous mudstone.
     3成藏组合包括三叠系-侏罗系烃源岩,侏罗系红色泥岩和下第三系-上第三系膏泥岩两套区域盖层和其它局部盖层,和三叠系-上第三系的砾岩、砂岩、粉砂岩和白云岩储层;
短句来源
     The results show that: 1) the globally distributed CORBs were mainly present in late Cretaceous; 2)the paleoenvironment of the CORBs is deep water of low latitude area in general; 3)the lithologies are mainly consisted of red shale, red limestone, red marlstone, red mudstone and red siliciclastic shale;
     通过对比,认为:1)这些全球分布的大洋红层主要出现在晚白垩世,2)一般分布在深水环境、低纬地区,3)在岩性上,主要由红色页岩、红色灰岩、红色泥灰岩、红色泥岩、红色硅质页岩几种岩性组成,4)有机碳含量普遍较低。
短句来源
     Tataaiertag formation is subdivided into upper member with red-brownish and red mudstone intercalated with siltstone and lower member with purple-red mudstone.
     塔塔埃尔塔格组两分,下段为紫红色泥岩,上段为红褐色、红色泥岩与粉砂岩不等厚互层。
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  “红色泥岩”译为未确定词的双语例句
     ON THE CONDITION OF WATER-BEARING SPACE DEVELOPMENT IN THE RED NUDSTONE APUIFER IN HENJYANJ BASIN
     衡阳红色泥岩含水层含水空间形成条件的初步研究
短句来源
     DIPODIDAE (RODENTIA, MAMMALIA) FROM THE LOWER MEadER OF XIANSHUIHE FORMATION IN LANZHOU BASIN, GANSU, CHINA
     甘肃兰州盆地咸水河组下段红色泥岩中的跳鼠化石
短句来源
     STUDY ON THE RULE OF VARIATION OF RED-MUDSTONE FROM JIANGXI ON HEATING
     江西红色泥岩加热变化规律研究
短句来源
     There is a suit of red glutenite layer and red shale layer in Sunjiawan group layer. And a suit of red glutenite and red shale alternating layers in upper Fuxin group layer and a suit of gray glutenite and gray shale layer in below Fuxin group layer, nipped with thin coal and bind.
     孙家湾组为一套红色砂砾岩与红色泥岩沉积,阜新组上部为红色泥岩与灰色砂砾岩互层,下部为灰色砂砾岩与灰色泥岩沉积,加薄煤层和炭质泥岩。
短句来源
     The differences between uranium-bearing and non-uranium sandstones and between red sandstone (claystone) and greenish sandstone can be determined by the gamma-ray spectroscopy (measuring U,Th and K) and XRF analysis (measuring As and Ba). Therefore, the prospecting of the sandstone-type uranium deposits in northern Sichuan can be concentrated in a certain ranse.
     通过伽马能谱法(测U,Th,K)和X射线荧光法(测As,Ba),区分含铀浅色砂岩和不含铀浅色砂岩,区分红色砂岩(红色泥岩)与浅色砂岩,缩小川北砂岩找铀矿的范围。
短句来源
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  相似匹配句对
     STUDY ON THE RULE OF VARIATION OF RED-MUDSTONE FROM JIANGXI ON HEATING
     江西红色泥岩加热变化规律研究
短句来源
     Red Sports Car
     红色跑车
短句来源
     Red
     38℃的红色
短句来源
     ON THE ROCK MECHANIC PROPERTICS OF MUDSTONES AND SANDSTONES IN THE MIDDLE PART OF SICHUAN RED BASIN
     川中红色泥岩岩石力学特性研究
短句来源
     A study on the creep properties of the mudstone
     泥岩蠕变性质的研究
短句来源
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  red mudstone
At Joggins, red mudstone units are about twice as abundant as the green mudstone units, yet the latter contain 26 charcoal horizons.
      
In the upper part of this slice, thin-bedded and slightly folded cherts alternate with red mudstone.
      
The lower six formations are dominantly red mudstone and yellowish-gray sandstone.
      


The red mudstone aquifer in Hengyang Basin consists of lacustrinefacies of late Cretaceous--Paleogene age with abundant fractures andcorrosional pore systems. Good ground water was found in this aquiferwith the pumping rates ranging from 300 to 700 cubic meters per day. Onthe basis of field investigation and experiment al data, this paper revealsthe mechanism of this phenomenon and the condition of water--bearingspace developrment. Sedimentary facies criteria for ground water predictionare also presented. Corrosional...

The red mudstone aquifer in Hengyang Basin consists of lacustrinefacies of late Cretaceous--Paleogene age with abundant fractures andcorrosional pore systems. Good ground water was found in this aquiferwith the pumping rates ranging from 300 to 700 cubic meters per day. Onthe basis of field investigation and experiment al data, this paper revealsthe mechanism of this phenomenon and the condition of water--bearingspace developrment. Sedimentary facies criteria for ground water predictionare also presented. Corrosional pores were formed from dissolution ofgypsum disseminated in rocks of salt lake sulphate subenvironment. Thedevelopment of corrosional pores and fractures closely associates withsedimentary facies in respect with structure, rhythmic layering and lithologicalcharacteristics of bed rocks. Sedimentary facies is the primary factor whichcontrols the distribution of good ground water. The secondary factor is theNeotectonic lifting which drives mudstone into an system open to theatmosphere, increasing ground water circulation.

衡阳红色泥岩含水层由晚白垩-早第三纪的湖相组成,含有比较丰富的溶孔水。本文围绕泥岩的富水机制论证了含水空间的形成条件,认为溶孔的形成主要是溶蚀分散状石膏所致,其分布规律受控于沉积环境的物质体现——沉积相;岩相特征是泥岩类富水的内因,外因则是新构造运动的抬升使岩体处于开放体系,从而增强了泥岩中地下水的循环条件。

The red mudstone acquifers in Hengyang Basin are relatively rich in groundwater contained in vugular pore space. In order to reveal the nature of the pheomenon, gypsum dissolution and calcite precipitation resulted from water-rock interaction are studied under the principles of thermodynamics. Processes of calcite precipitation are discussed in three aspects_1 common ion effect, proton transfor mation and complex formation.

衡阳红色泥岩含水层含有比较丰富的溶孔水,水岩作用导致石膏溶解及方解石析出。本文围绕水中碳酸钙沉淀达一现象,运用热力学分析原理,从同离子效应、质子转移理论以及成络作用三个方面分析了红层溶孔水碳酸钙沉淀反应的三种作用,试图揭示这一现象的水文地球化学本质。

Most geologists used to consider that the Kedoushan Formation belongs to theUpper Jurassic based on its lithogical character and fossils, and that it was equiv-alent to the famous Kienteh Group in the Shouchang Region, Zhejiang Prov-ince. The present paper considers that the Kedoushan Formation is a series ofstrata with a time span from Upper Jurassic to Lower Cretaceous. It can be di-vided into three parts according to lithological character; the upper part consist-ing of volcanic rocks;the middle part consisting...

Most geologists used to consider that the Kedoushan Formation belongs to theUpper Jurassic based on its lithogical character and fossils, and that it was equiv-alent to the famous Kienteh Group in the Shouchang Region, Zhejiang Prov-ince. The present paper considers that the Kedoushan Formation is a series ofstrata with a time span from Upper Jurassic to Lower Cretaceous. It can be di-vided into three parts according to lithological character; the upper part consist-ing of volcanic rocks;the middle part consisting of red-color sedimentary rocks;and the lower part consisting of greyish-green sedimentary rocks. They arenamed Beds a, b and c respectively in ascending order at the section of Wai-shan--Madaishan in this region. Both Beds a and b are abundantly fossilife-rous. The charophytes in the assemblage of Bed a consist of Aclistochara, Poro-chara, Latochara, Sphaerochara, Nodosoclavator, etc. Some of these species havebeen found (or are similar to those) from Kimmeridgian of Northwest Germanyand from the Morrison Formation of West America (Madler, 1952; Peck, 1937,1957), such as Aclistochara latisulcata Peck, A. obovata Peck, Porochara cf. kim-meridgensis, (Madler), P. cf. raskvae (Madler), Latochara cf. latitruncata (Peck),Sphaerochara cf. verticillata (Peck), S. cf. latifasciata (Peck), etc. The assem-blage resembles those of the Suining Formation, Upper Shaximiao Formation andPengleizhen Formation in Sichuan Province (Liu Junying, 1982). It also resem-bles those of the Xiangtan Formation and Datonghe Formation in the Xiningand Minhe Basins in Qinghai Province (Hao Yichun et al.,1983). Especially,thegenus Aclistochara is abundantly found in those regions. Some species of Stella-tochara spp. have never been found from the Cretaceous and younger strata.Therefore, based upon this charophytes assemblage, the author thinks that Bed abelongs to Late Jurassic age. A huge amount of Clavatoraceae (Charophyta) is found in Bed b, consist-ing of Flabellochara, Nodosoclavator.The genus Mesochara is also abundant in thisassemblage. Flabellochara is widely distributed in Early Cretaceous age allover the world, representing one of the index fossils from the Wealden Stage to the Aptian Stage. This indicates that Bed b of the Kedoushan Formationcertainly belongs to Early Cretaceous age. In this region, the upper volcanic rock usually overlies the different bedsof the lower deposit, and the volcanic rock mostly overlies Bed a directly. Theauthor can determine that there had occurred an elevation and that Bed b inmost sections had been eroded before the volcanic eruption of Bed c. According to the charophyte assemblages and the sedimentary character, asedimentary gap is not appreciable in this region between the Jurassic and Cre-taceous. A boundary between Upper Jurassic and Lower Cretaceous charophy-tes can be demarcated in the Kedoushan Formation. Only Bed a belongs to theUpper Jurassic.

繁昌地区蝌蚪山组原定为晚侏罗世。本文根据轮藻化石群的研究结果并结合岩石特征,认为该组可以分为三部分。下部杂色砂泥岩产Aclistochara,Porochara,Sphaerochara,Latocha-ra等轮藻化石组合为a段,归晚侏罗世;中部产Flabellochara,Mesochara轮藻化石组合的红色泥岩为b段;上部火山岩为c段,b、c两段时代均属早白垩世。本文着重讨论了a、b两段地层中轮藻化石组合特征及有关问题。本区这两个轮藻化石组合的发现对我国东南地区晚中生代火山岩系的划分对比有所裨益。本文共记述了轮藻化石10属27种,其中有9个新种,4个相似种。

 
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